En poursuivant votre navigation sur ce site, vous acceptez l’utilisation de cookies à des fins de mesure d’audience et pour vous permettre d’échanger sur les réseaux sociaux.

Causses & Cévennes - sud Massif Central

Causses Cévennes

Vacation in the Gorges du Tarn, Causses & Cevennes

Traditionnal limestone architecture on the Causses & in Gorges

L'architecture caussenardeThis typical limestone architecture can be found on the highlands (Causse Méjean, Causse Noir and Causse de Sauveterre) and the canyons (Gorges du Tarn, Gordes de la Jonte and Lot valley).

INTRODUCTION CAUSSENARD ARCHITECTURE

At the immense limestone table-plateaus, the so-called Causses you become aware of a wide open horizon, slightly undulated  with a average height close to thousand meter.
Here rain comes down without streaming,  absorbed by the mass of limestone. It's the land of sheep, sheep for meat et sheep for milk, for the Roquefort dairies.

col de MontmiratLimestone is an easy to win bedrock . Its breaking in strata of very different thickness. These layers are serviceable in their natural form. Thin layers generates flat ones for masonry, roof- and floor-slating.  
Thick layers and big blocks are providing angle-stones, cross-connection-stones, lintels, door- and windowframes and the eventual protuding stones for futur neighbour construction(s) in times of demographical or economical highlights.

The early disafforestation of the highlands (already in the stone age and mostly terminated by the mobile glass industry from Milau) are responsible for the absence of wood in general and timber in particular.
That's why everything even rafter and interfloors are realised in stone,  rooms, floors and roofs are vault-constructions. THE caracteristic of causenard architecture.

The limestone architecture in the valley and sticked to the giant canyons which border the Causses is different at some points, due to the geographical differences:

  • the presence of water
  • a vegetation of beech, pine, oak and brushwood
  • the natural protection of the rocky walls behind
  • the scarceness of flat terrain.
    Although it’s the same geological material the architectural characteristics differs as much as those in the contact-zones with granite or schist.

THE VAULTED STRUCTURE OF CAUSSENARD CONSTRUCTIONS

grange voutée, causse MéjeanThe most of the farms at the Causses count two main vaults : the interfloor and the arched roofing.
The supporting vault, the lowest one between the ground level and the first floor is a flattened arch, this type of vault exerces his main forces horizontal which permit to overstrain a relative wide breadth.

The superior vault is a so-called broken one, consisting of two half arches in support of eachother.The oblique pression of this vault equilibrates the sidewards pression of the lower one.
Their resultant is absorbated by the the part of the wall were the broken vault begins.
To compensate the horizontal forces of the construction, this superior vault is made quit high.
This system realizes a big volume which can easily lodge a third level when required with a wooden floor in between.

Normally the vaults are built out of unselected stones (pierre tout venant) like the walls. Only churches and other buildings of (public) importance are made out of hewd stones.
bergerie causse MéjeanThe vault-shape offers a numerous possibilities to variate, even while respecting the forces. A vault is set up at both sides of a wooden mould, which is moving forwards with the advancing of the work.

The upper side of the lowest arch is filt up whith stones, earth, straw and other debris and is carrying the tiled floor with the big flat limestone slabs of the kitchen/living.

Intersections of the vaults and al the openings have to be solid and rigid for not to compromise the coherence of the construction, which is transmitted by every stone to his neighbours.
Also the lateral constructions with a half-vault roofconctruction are giving solidity towards building, like the buttresses (les enculos) and the supporting arches (les arcs d’épaulement).retour ...

THE FACADES

The principal gables are to be SEEN, to invite visitor and sunshine, to be the card of the habitants.little farm, col de Montmirat
Also for coming in for light and visitors they're useful.
There are two types of fronts:
The gable-wall -one: façade en mur pignon

evier calcaireBecause the gable walls don't  support the main weight of the vault   there can be made door and windows quit easily without compromising the solidsity of the building .
This is the simplest way, used when the house is built perpendicalar at the slope. The disadvantage is that it don't permit the daylight to come deep in to the house.

The long-side one: La façade sur le mur de long pan also called the gutter wall: mur gouttereau. In this type the openings have to been realised by construction of cross-vaults ancred in the main one.

All the openings are lining up in a axe of cross-vaults, which receives the pushing force of the heayvy roof leading the resultant at either side in the very thick wall beneath.
In both types of farm(mas) the lowest and higher level only communicate by outside, while to force a gap in the supporting vault was impossible.

The main door of the kitchen in both cases can be reached by steps built over a vault with a paved platform on it. This sometimes covered space   is complementary living space when the climate permits it.

THE ROOF

The gradient of the roof, between 40 and 60 % is determinated by the upper vault and the height of the wall.

The tangent of the upper vault is filt up with a layer of earth and covered with triangle little stiffy stones to hold the heavy limestone slabsby their own weight.

At the base of the roof the largest slabs (les gouttiers-the gutters) hanging over the walls to protect them.
Then their dimensions decrease whith each higher range til the top, formed by flat placed slates.

In the type of ‘façade à long pan’, the different square roofparts have to been integrated in the angle by round-formed slate-ranges. These so called noues (knot) en arrondis are masterpieces.

façade à ChabrièreTo avoid snow wind and water to penetrate the roof each slab has to be covered 2/3 of their surface by the uppers. The weight (200 à 250 kg / m2, or even more) is a welcome force to block the masonry of the vault.
So it's extremely stupid to undo one side of the roof, out of equilibrium the building will collapse.
Certain more recent roofs are only supported by vaulted arches of stone in stead of a whole vault.These arches are connected by timber. The slabs also are resting at timber with a very little gradient to avoid them to slide down.
But with the generalization of slatestone slates which can be nailed this problem is solved..

 

 

THE OPENINGS

Windows and doors are mostly made at the sunny side.
Placed in the longest side of the building they are directly under the eaves with a perpendicular little vault to the main one.
This so-called lucarne is an other characteristic of limestone architecture.
Otherwise ,if the orientation of a gablewall is to the sunshine then the openings are made there.

ARCHITECTURAL SURROUNDINGS OF A MAS (farmhouse)

Contrary to the architecture of the limestone valleys, or schist cevennes with their close knot hamlets, here the most annexes are juxtaposed.
Because space is available, only to share walls  or to improve a buildings solidity some annexes share walls with the main building or eachother.
The different elements of a caussenard mas are:

  • the main house, sheepfold and living
  • the bread-oven in the courtyard or integrated in the chimney gable with it's entrance in the chimney.
  • pigsty, straw-loft, hay-loft, watertank(s)
  • storage buildings for harvest, tools and beast
  • The threshing-floor to threat the cereals which florish well at the Causses.In general in touch with the straw-lof.
  • Some farms have a pigeon-tower, characteristic for a cereals region, only after the Revolution allowed to everyone
  • The constructed space is spread out over the environment:
  • Garden, meadows, and tracks bordered by stone walls, terrace-walls to hold back the fertile earth
  • walls to seperate properties
  • Little shelters for shepherds and tools in the middle of the fields
  • The lavognes, little clay-lined depressions, impermeable filled up with rain-water, the only water available till 1965
  • Dolines, cultivated former waterholding depressions with red fertile earth,or collapsed rockroof of a shallow underground cavity.
  • The deep ones also originates by the dissolving calciumcarbonate of the limestone rainwater rock which hollows out easily.
  • Caverns and cavities, an amazing underground world, all over the causses.
  • The well  nearby the kitchen or even in it. Every mas collected the maximum of rain water in its eaves which was stored in a big watertank ( la citerne).
  • Heaps old stones cleared from the field the so called clapas.
  • The tumulus, very old graves under a base of earth under a heap of stones, a lot of neolithic dolmens and other prehistorian 'architecture' like menhirs.

The landscape is completed with a very special flore  (sometimes making part of architectural elementsgrasses, shrubs, trees and a lot of protected flowers) and faune like the griffon vulture taking habitat in the geological architecture, the nature of the Causses.

THE LIMESTONE ARCHITECTURE IN THE VALLEY

In the valley certains components remains the same, but a lot also differs related to presence the relief and different climatic conditions.
Beatiful little properties sticked to the slope are settled near a source. They cultivated fruit (pears & apples), grapes for wine and kept little goat/sheep- herds.
The lowest part of each house,the cave is hewed out of thebed-rock, laying partially in it, serves to make wine, to preserve fruit and contains a watertank.

Beside there is another cave for donckey, mule, pig, a few goats and sheep.
At the first floor lies the kitchen, the living, to enter by steps and a little platform.
The second floor whith timber roof or stonen vault is for storing branches with leaves or other things, herer hay is rare.

In the dolomitic sector in the gorges themselves, ruiniform reliefs bordering the plateaus, the habitat has a troglodyte caracter: the rocky walls were integrated in the houses. They are completely integrated in the environment of ledges that overhang the valley.
Natural caves are fitted up as sheep and goatsfold, shelter, shed etc

The presence of water and passages or bridges are in this country -of difficult acces, the main reasons to settlement ;farms, hamlets or even villages. Malbosc

Construction added during centuries are purely due to the presence of:
water to cultivate*
fertile land
a relative flat area
rocks favorable to defense or construction
proximity of communication tracks.
In this close knot-type of hamlets and villages each house lays in a very narrow street with a window towards the valley..
* (at the most arid areas only sheepholding was possible, in dry years the lavognes and watertanks were dry and empty, so the had to go down the gorges)

THE ZONES OF TRANSITION

schiste-slatestoneThe quit homogene architecture of the valleys and plateaus changes suddenly where other geological matearial occurs.
In the Tarnon-valley  for instance, the sources appear were the permeables layers of limestone meet the impermeable schist . This has had immediately  its reflection in a combinated architecture with stonen vaults as well as timber roof and floors.
A bit further direction cévennes schist starts to be the predominant material : only  angle-stones and  the stones around door- and windowframes and are hewn in pale limestone. The resistance of schist to pressure is inferior to that of limestone, granite or fraidonite.

At the littles  lime-stone plateaus separated from the causses the material is of an other nature, an other geological niveau. Here you can find caussenard architecture co-existing with rafter constructions.
Also in the marlstone valleys of theValdonnez the architecture has his own particularities like the square pigeon-towers;In the region of the Bondons the series of big lucarnes*  will please you.  (*lucarne : little window in cross vault in the roof )

In the contact zone with granite du mont Lozère both  materials are mixed up in an amazing combination of characteristics of both architectures, like a caussenard model all realised in granite.

Castelbouc, gorges du TarnTO VISIT:

  • le Causse Noir, dolomitic reliefs: Montpellier le Vieux
  • Causse Larzac
  • Causse the Sauveterre:  highest point Point sublime, land of the menhirs
  • Causse Méjean (mejan:in the middle) ,highest point :Roc des Hourtous, le hameau de l'hom, archaeoligical museum at La parade: "la Borie"
  • Drigas, Nîmes le vieux,
  • Arcs de St. Pierre
  • Aven Armand
  • the "arcs de St. pierre
  • Le Rozier (vultures)

 

 

OPENINGS

Windows and doors are mostly made at the sunny side.
Placed in the longest side of the building they are directly under the eaves with a perpendicular little vault to the main one.
This so-called lucarne is an other characteristic of limestone architecture.
Otherwise ,if the orientation of a gablewall is to the sunshine then the openings are made there. .

ARCHITECTURAL SURROUNDINGS OF A 'MAS'

Contrary to the architecture of the limestone valleys, or schist cevennes with their close knot hamlets, here the most annexes are juxtaposed.
Because space is available, only to share walls  or to improve a buildings solidity some annexes share walls with the main building or eachother.
The different elements of a caussenard mas are:

  • the main house, sheepfold and living

  • the bread-oven in the courtyard or integrated in the chimney gable with it's entrance in the chimney.

  • pigsty, straw-loft, hay-loft, watertank(s)

  • storage buildings for harvest, tools and beast

  • The threshing-floor to threat the cereals which florish well at the Causses.In general in touch with the straw-loft

  • Some farms have a pigeon-tower, characteristic for a cereals region, only after the Revolution allowed to everyone

    The constructed space is spread out over the environment:

  • Garden, meadows, and tracks bordered by stone walls

  • terrace-walls to hold back the fertile earth

  • walls to indicate properties

  • Little shelters for shepherds and tools in the middle of the fields

  • The lavognes, little clay-lined depressions, impermeable filled up with rain-water, the only water available till 1965.

  • Dolines, cultivated former waterholding depressions with red fertile earth,or collapsed rockroof of a shallow underground cavity.
    The deep ones also originates by the dissolving calciumcarbonate of the limestone rainwater rock which hollows out easily.

  • Caverns and cavities, an amazing underground world
    all over the causses.

  • The well  nearby the kitchen or even in it. Every mas collected the maximum of rain water in its eaves which was stored in a big watertank ( la citerne).

  • Heaps old stones cleared from the field the so called clapas.
    The tumulus, very old graves under a base of earth under a heap of stones, a lot of neolithic dolmens and other prehistorian 'architecture' like menhirs.

    The landscape is completed with a very special flore  (sometimes making part of architectural elementsgrasses, shrubs, trees and a lot of protected flowers)
    and faune like the griffon vulture taking habitat in the geological architecture, the nature of the Causses.

THE LIMESTONE ARCHITECTURE IN THE VALLEY

In the valley certains components remains the same, but a lot also differs related to presence the relief and different climatic conditions.
Beatiful little properties sticked to the slope are settled near a source. They cultivated fruit (pears & apples), grapes for wine and kept little goat/sheep- herds.
The lowest part of each house,the cave is hewed out of thebed-rock, laying partially in it, serves to make wine, to preserve fruit and contains a watertank.

Beside there is another cave for donckey, mule, pig, a few goats and sheep.
At the first floor lies the kitchen, the living, to enter by steps and a little platform.
The second floor whith timber roof or stonen vault is for storing branches with leaves or other things, herer hay is rare.

In the dolomitic sector in the gorges themselves, ruiniform reliefs bordering the plateaus, the habitat has a troglodyte caracter: the rocky walls were integrated in the houses. They are completely integrated in the environment of ledges that overhang the valley.
Natural caves are fitted up as sheep and goatsfold, shelter, shed etc

The presence of water and passages or bridges are in this country -of difficult acces, the main reasons to settlement ;farms, hamlets or even villages. Malbosc

Construction added during centuries are purely due to the presence of:
water to cultivate*
fertile land
a relative flat area
rocks favorable to defense or construction
proximity of communication tracks.
In this close knot-type of hamlets and villages each house lays in a very narrow street with a window towards the valley..
* (at the most arid areas only sheepholding was possible, in dry years the lavognes and watertanks were dry and empty, so the had to go down the gorges)

THE ZONES OF TRANSITION


schiste-slatestoneThe quit homogene architecture of the valleys and plateaus changes suddenly where other geological matearial occurs.
In the Tarnon-valley  for instance, the sources appear were the permeables layers of limestone meet the impermeable schist . This has had immediately  its reflection in a combinated architecture with stonen vaults as well as timber roof and floors.
A bit further direction cévennes schist starts to be the predominant material : only  angle-stones and  the stones around door- and windowframes and are hewn in pale limestone. The resistance of schist to pressure is inferior to that of limestone, granite or fraidonite.

At the littles  lime-stone plateaus separated from the causses the material is of an other nature, an other geological niveau. Here you can find caussenard architecture co-existing with rafter constructions.
Also in the marlstone valleys of theValdonnez the architecture has his own particularities like the square pigeon-towers;In the region of the Bondons the series of big lucarnes*  will please you.  (*lucarne : little window in cross vault in the roof )

In the contact zone with granite du mont Lozère both  materials are mixed up in an amazing combination of characteristics of both architectures, like a caussenard model all realised in granite.

Organising a visit :

You can ask the Tourist Office in Meyrueis for more general information
To know some more or in detail about the Gorges and Causses:Castelbouc, gorges du Tarn

  • le Causse Noir, dolomitic reliefs: Montpellier le Vieux

  • Causse Larzac

  • Causse the Sauveterre:  highest point Point sublime, land of the menhirs

  • Causse Méjean (mejan:in the middle) ,highest point :Roc des Hourtous, le hameau de l'hom, archaeoligical museum at La parade: "la Borie"

  • enceinte de Drigas, Nîmes le vieux,

  • Arcs de St. Pierre

  • Aven Armand

  • the "arcs de St. pierre

  • Le Rozier (vultures)